Journal articles on the topic 'Olary Domain'

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1

Law, Steve, and Stephen Busuttil. "Geophysics of the Kalkaroo prospect, Olary Domain, South Australia." ASEG Extended Abstracts 2003, no. 3 (December 2003): 121–26. http://dx.doi.org/10.1071/asegspec12_10.

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2

Griessmann, Martin, Andreas Schmidt Mumm, Thomas Seifert, and Colin Conor. "The Mt. Mulga barite–magnetite–copper–gold mineralisation, Olary Domain, South Australia." Journal of Geochemical Exploration 106, no. 1-3 (July 2010): 110–20. http://dx.doi.org/10.1016/j.gexplo.2009.11.008.

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3

Pepper, M. A., and P. M. Ashley. "Volcanic textures in quartzo‐feldspathic gneiss of the Willyama Supergroup, Olary Domain, South Australia." Australian Journal of Earth Sciences 45, no. 6 (December 1998): 971–78. http://dx.doi.org/10.1080/08120099808728451.

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4

Ashley, P. M., B. G. Lottermoser, and J. M. Westaway. "Iron-formations and epigenetic ironstones in the Palaeoproterozoic Willyama Supergroup, Olary Domain, South Australia." Mineralogy and Petrology 64, no. 1-4 (March 1998): 187–218. http://dx.doi.org/10.1007/bf01226569.

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5

Clark, Christopher, and Patrick James. "Hydrothermal brecciation due to fluid pressure fluctuations: examples from the Olary Domain, South Australia." Tectonophysics 366, no. 3-4 (May 2003): 187–206. http://dx.doi.org/10.1016/s0040-1951(03)00095-7.

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6

Hills, Q. G., P. G. Betts, and G. S. Lister. "Geophysical interpretation and modelling of the Olary Domain under cover: A hidden inverted rift system." Australian Journal of Earth Sciences 50, no. 4 (August 2003): 633–44. http://dx.doi.org/10.1046/j.1440-0952.2003.01017.x.

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7

Griessmann, Martin, Andreas Schmidt Mumm, Thomas Seifert, and Colin Conor. "The mineralising system of the Mt. Mulga barite–magnetite–Cu–Au mineralisation, Olary Domain, South Australia." Journal of Geochemical Exploration 101, no. 1 (April 2009): 44. http://dx.doi.org/10.1016/j.gexplo.2008.12.059.

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8

CLARK, C., A. SCHMIDT MUMM, and K. FAURE. "Timing and nature of fluid flow and alteration during Mesoproterozoic shear zone formation, Olary Domain, South Australia." Journal of Metamorphic Geology 23, no. 3 (April 2005): 147–64. http://dx.doi.org/10.1111/j.1525-1314.2005.00568.x.

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9

Clark, Chris, Ben Grguric, and Andreas Schmidt Mumm. "Genetic implications of pyrite chemistry from the Palaeoproterozoic Olary Domain and overlying Neoproterozoic Adelaidean sequences, northeastern South Australia." Ore Geology Reviews 25, no. 3-4 (October 2004): 237–57. http://dx.doi.org/10.1016/j.oregeorev.2004.04.003.

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10

Page, R. W., C. H. H. Conor, B. P. J. Stevens, G. M. Gibson, W. V. Preiss, and P. N. Southgate. "Correlation of Olary and Broken Hill Domains, Curnamona Province:Possible Relationship to Mount Isa andOther North Australian Pb-Zn-Ag-Bearing Successions." Economic Geology 100, no. 4 (June 1, 2005): 663–76. http://dx.doi.org/10.2113/gsecongeo.100.4.663.

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11

Page, R. W., C. H. H. Conor, B. P. J. Stevens, G. M. Gibson, W. V. Preiss, and P. N. Southgate. "Correlation of Olary and Broken Hill Domains, Curnamona Province: Possible Relationship to Mount Isa and Other North Australian Pb-Zn-Ag-Bearing Successions." Economic Geology 100, no. 4 (June 1, 2005): 663–76. http://dx.doi.org/10.2113/100.4.663.

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12

Anderson, Martin. "Estonian Composers (combined Book and CD Review)." Tempo 59, no. 232 (April 2005): 60–66. http://dx.doi.org/10.1017/s0040298205210161.

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Ancient Song Recovered: The Life and Music of Veljo Tormis, by Mimi S. Daitz. Pendragon Press, $54.00/£36.00.The Works of Eduard Tubin: Thematic-Bibliographical Catalogue of Works by Vardo Rumessen. International Eduard Tubin Society/Gehrmans Musikförlag, E.57.TORMIS: ‘Vision of Estonia’ II. The Ballad of Mary's Land; Reflections with Hando Runnel; Days of Outlawry; God Protect Us from War; Journey of the War Messenger; Let the Sun Shine!; Voices from Tammsaare's Herdboy Days; Forget-me-not; Mens' Songs. Estonian National Male Choir c. Ants Soots. Alba NCD 20.TORMIS: ‘Vision of Estonia’ III. The Singer; Songs of the Ancient Sea; Plague Memory; Bridge of Song; Going to War; Dialectical Aphorisms; Song about a Level Land; We Are Given; An Aboriginal Song; The Estonians' Political Parties Game; Song about Keeping Together; Martinmas Songs; Shrovetide Songs; Three I Had Those Words of Beauty. Estonian National Male Choir c. Ants Soots. Alba NCD 23.TAMBERG: Cyrano de Bergerac. Soloists, Orchestra and Chorus of Estonian National Opera c. Paul Mägi. CPO 999 832-2 (2-CD set).ROSENVALD: Violin Concerto Nos. 11 and 2, Quasi una fantasia2; Two Pastorales3; Sonata capricciosa4; Symphony No. 35; Nocturne6. 1,2Lemmo Erendi (vln), Tallinn CO c. Neeme Järvi, 2Estonian State SO c. Jüri Alperten; 3Estonian State SO c. Vello Pähn; 4Valentina Gontšarova (vln); 56Estonian State SO c. Neeme Järvi. Antes BM-CD 31.9197.DEAN: Winter Songs. TÜÜR: Architectonics I. VASKS: Music for a Deceased Friend. PÄRT: Quintettino. NIELSEN: Wind Quintet. Berlin Philharmonic Wind Quintet, with Daniel Norman (tenor), c. Hermann Bäumer. BIS-CD–1332.TULEV: Quella sera; Gare de l'Est; Adiós/Œri Ráma in memoriam; Isopo; Be Lost in the Call. NYYD Ensemble c. Olari Elts. Eesti Raadio ERCD047.ESTONIAN COMPOSERS I: MÄGI: Vesper.1 KANGRO: Display IX.2 SUMERA: Shakespeare's Sonnets Nos. 8 & 90.3TAMBERG: Desiderium Concordiae.4 TULEV: String Quartet No. 1.5 EESPERE: Glorificatio.6 TORMIS: Kevade: Suite.71Estonian National SO c. Aivo Välja; 24NYYD Ensemble c. Olari Elts; 3Pirjo Levadi (soprano), Mikk Mikiver (narrator), Estonian National Boys' Choir, Estonian National SO c. Paul Mägi; 5Tallinn String Quartet; 6Kaia Urb (sop), Academic Male Choir of Tallinn Technical University c. Arvo Volmer; 7Estonian National SO c. Paul Mägi Eesti Raadio ERCD 031.ESTONIAN COMPOSERS II: TULVE: Traces.1 TALLY: Swinburne.2 KÕRVITS: Stream.3 STEINER: Descendants of Cain.4 KAUMANN: Long Play.5 LILL: Le Rite de Passage.6 SIMMER: Water of Life.71,5,6NYYD Ensemble c. Olari Elts; 2Ardo-Ran Varres (narrator), Iris Oja (sop), Alar Pintsaar (bar), Vambola Krigul (perc), Külli Möls (accordion), Robert Jürjendal (elec guitar); 3Virgo Veldi (sax), Madis Metsamart (perc); 4The Bowed Piano Ensemble c. Timo Steiner; 7Teet Järvi (vlc), Monika Mattieson (fl). Eesti Raadio ERCD032.ESTONIAN COMPOSERS III: GRIGORJEVA: Con misterio;1On Leaving. SUMERA: Pantomime; The Child of Dracula and Zombie. 1Tui Hirv (sop), 1Iris Oja (mezzo), 1Joosep Vahermägi (ten), 1Jaan Arder (bar), Hortus Musicus c. Andres Mustonen. Eeesti Raadio ERCD 045ESTONIAN COMPOSERS IV: KRIGUL: Walls.1 JÜRGENS: Redblueyellow.2 KÕRVER: Pre.3 KOTTA: Variations.4 SIIMER: Two Pieces.5 KAUMANN: Ausgewählte Salonstücke.6 AINTS: Trope.7 STEINER: In memoriam.81,6New Tallinn Trio; 2Liis Jürgens (harp); 3,8Voces Musicales Ensemble c. Risto Joost; 4Mati Mikalai (pno); 5Mikk Murdvee (vln), Tarmo Johannes (fl), Toomas Vavilov (cl), Mart Siimer (organ); 7Tarmo Johannes (fl). Eeesti Raadio ERCD 046.BALTIC VOICES 2: SISASK: Five songs from Gloria Patri. TULEV: And then in silence there with me be only You. NØRGÅRD: Winter Hymn. GRIGORJEVA: On Leaving (1999). SCHNITTKE: Three Sacred Hymns. Estonian Philharmonic Chamber Choir c. Paul Hillier. Harmonia Mundi HMU 907331.SCHNITTKE: Concerto for Chorus; Voices of Nature. PÄRT: Dopo la vittoria; Bogoróditse Djévo; I am the True Vine. Swedish Radio Choir c. Tõnu Kaljuste. BIS-CD-1157.PÄRT: Es sang vor langen Jahren; Stabat Mater; Magnificat; Nunc Dimittis; My Heart's in the Highlands; Zwei Sonatinen; Spiegel im Spiegel. Chamber Domaine; Stephen de Pledge (pno), Stephen Wallace (counter-ten), Choir of St Mary's Cathedral, Edinburgh c. Matthew Owens. Black Box BBM1071.
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13

Everaerts, Michel, and Jean-Louis Mansy. "Le filtrage des anomalies gravimetriques; une cle pour la comprehension des structures tectoniques du Boulonnais et de l'Artois (France)." Bulletin de la Société Géologique de France 172, no. 3 (May 1, 2001): 267–74. http://dx.doi.org/10.2113/172.3.267.

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Abstract The geology of the Boulonnais has been well studied since the early part of the last century [Gosselet and Bertaut, 1873; Olry, 1904; Pruvost and Delepine, 1921]. Extensive coal exploration added substantially to the general understanding of the geology of the region but as outcrop is poor, many questions remain. Gravity methods used in the analysis of geological structures have had a long and successful history in helping to study the earth's crust for scientific and applied objectives. Regional gravity data are particularly useful in mapping geographic distribution and configuration of density contrast of rocks. Previous gravity research shows the main trends of the structure. In most cases the regional Bouguer gravity hides the relationship between the geology and the shape of the anomaly caused by the perturbing body. New information can be obtained by filtering the maps. The purpose of filtering a map is to remove unwanted characteristics and enhance desirable characteristics that are diagnostic for the geology. Because of their simple mathematical forms, most potential field filters are in the spectral domain. It is advisable to transform the original unfiltered field to the spectral domain, apply the filter, then transform the filtered map back to the spatial domain for use in the interpretation. Several spectrally filtered versions of the original gravity map are used in this regional interpretation. In the case of the Boulonnais the most useful filters have been the horizontal component and the first vertical derivative. In the first instance computing the horizontal gradients of the gravity field permits us to localise the limit of the blocks and then the fault positions. The gravimetric field above a vertical contact of rock with different density shows a low on the side of the low density rocks and a high on the side of the high density rocks. The inflection point is located just on the contact of the two types of rocks. This contact can be outlined by locating the maxima of the horizontal gradient. In the case of a low dipping contact maxima stay close to the contact, but are displaced down dip. In the second instance the first vertical derivative acts as a booster for the short wavelength; this attenuates or destroys the effect of the regional field. The resulting map shows a better structure because in complex areas they give a better definition of the different bodies by separating their effects. In the case of the Boulonnais the first vertical derivative allows us to distinguish the depressed region from the uplifted one. The structural evolution of the Boulonnais-Artois area includes two main extensional events in the late Palaeozoic-early Cretaceous interval and an inversion in mid-late Palaeocene time. The new gravity data in combination with recent field and published data have provided a new insight into the structure of the Boulonnais-Artois area and a new interpretation is proposed. -- Fault patterns are oriented 110N and 040N in the Boulonnais and 140N in Artois areas. -- The linkage between the faults shows a relay geometry with transfer zones [cf. Morley et al., 1990 and Pea-cock and Sanderson, 1994]. The best example is located between Sangatte (near the tunnel) and Landrethun faults where overlapping synthetic faults with a relay ramp are imaged. -- There is no major continuous fault zone but a complex en echelon fault system. -- Linkage between Boulonnais and Artois fault is not well constrained. An important discontinuity between the two regions is apparent. This model underlines the importance of overlapping fault tips with the generation of transfer zones. These structures are also known in the Wessex and Weald basins [Stoneley, 1982; Chadwick, 1993] where heritage and inversion are significant.
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14

VАRENTSOVA, Larisa Yu. "PALACE AGRICULTURE IN RUSSIA IN THE 17TH CENTURY." Tyumen State University Herald. Humanities Research. Humanitates 6, no. 3 (2020): 118–36. http://dx.doi.org/10.21684/2411-197x-2020-6-3-118-136.

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Throughout the 17th century, the Palace economy developed dynamically in the Royal fiefdoms, which by the middle — the second half of the 17th century were characterized by high profitability. The Palace lands provided the Romanov House with everything it needed. The components of the Palace economy included agriculture, fishing grounds, and manufacturing facilities. At the same time, the Royal manufactories were not numerous, the fishing grounds were not in all the sovereign’s fiefdoms, only agriculture dominated everywhere. The relevance of this work lies in studying the historical experience of socio-econo­mic and political development of the Russian state in the 17th century. The purpose of the article is to consider Palace agriculture in Russia in the 17th century. The methodological basis of the study relies on the principles of historicism and scientific objectivity. The author has used the works by russian pre-revolutionary historians V. N. Tatishchev, S. M. Solovyov, and M. Baranovsky, as well as the works of researchers of the soviet and post-soviet periods S. I. Volkov, V. I. Buganov, V. A. Korostelev, and A. V. Topychkanov. The novelty of the research consists in the introduction of new historical sources into scientific circulation. The source database consists of the unpublished office documents from the Armory chamber fund 396, the Palace department fund 1239 of the Russian State Archive of Ancient Acts (RGADA, Moscow), as well as from the rare handwritten and old-printed books fund of the Moscow state United art historical, architectural and natural landscape museum-reserve. Among the published sources, we can distinguish a group of office documents. These are census, parish, and expense books of orders of Secret Affairs and the Grand Palace. In addition, the author has used the historical and geographical materials of the 17th — early 18th century from the books of the Discharge Order and the memoirs by the german traveler A. Oleary. The results show the place of Palace agriculture in the economy of the Tsar’s domain in Russia in the 17th century. The author has identified the main directions in the development of agriculture on the territory of the Palace fiefdoms. Having studied the attempt to modernize the Palace agriculture during the reign of Tsar Alexei Mikhailovich and to use the best european experience, this research highlights the significance of the Secret Affairs Order, which was in charge of many agricultural objects in the second half of the 17th century; their geographical coordinates are indicated. The author reveals the main features of the development of Palace grain farming, horticulture, animal husbandry, poultry farming, and beekeeping. The examples of farming in some Tsar’s villages of the Moscow Region showcase the ways of providing labor for the main objects of agriculture in the Tsar’s domain. The agricultural products from the Royal fiefdoms were intended for the Royal family. To a lesser extent, they were sent for sale on the domestic market. Different Royal fiefdoms specialized in particular fields. Namely, Izmailovo, Chashnikovo, Alekseevskoye, Stepanovskoye, Ekaterininskaya Grove, and Yermolino Palace villages near Moscow supplied rye, oats, wheat, hops, flax, and hemp. Grape, fruit, and mulberry orchards were bred in Chuguev, Astrakhan, Bryansk, and the Moscow Region. Russian and German specialists were involved in their service. The Palace villages Pachino, Alekseevskoe, Stepanovski, Ermolino, situated near Moscow, and the villages Lyskovo and Murashkino near Nizhny Novgorod were the centres of the Palace livestock. Tsar’s apiaryies were in Karpovka, Volnovsky, Kharkiv, Chuguyev, Olesinska, and Hotnichescom counties. Palace agriculture was served using the forced labor of palace peasants and posadsky people, soldiers, archers, while only small amounts of hired labor were involved.
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15

"Determination of Glycolipids, Sulfolipid and Phospholipids in the Thylakoid Membrane." Zeitschrift für Naturforschung C 48, no. 7-8 (August 1, 1993): 623–31. http://dx.doi.org/10.1515/znc-1993-7-816.

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Abstract Determination of binding of antibodies to lipids onto the surface of the thylakoid mem­ brane, before and after the removal of the CF1-complex with sodium bromide, showed that in the immediate vicinity of CF1 sulfolipid and monogalactolipid occur in higher concentration and are therefore arranged in domains. The m olar ratio of the CF1-complex to glycolipids was determined in Nicotiana tabacum chloroplasts of different structure. Thus, in the chlorophyll-deficient tobacco mutants N. tabacum Su/su and Su/su var. Aurea, the molar ratio of CF1/ monogalactolipid is the same and found to be 1:570. The structure of the lamellar system in these mutants is characterized by a higher ratio of stroma lamellae to grana stacks when compared to the green wild type. In the wild type the ratio CF1/monogalactolipid is 30 per cent larger (1 :740). In contrast to this the m olar ratio CF1/sulfolipid and CF1/digalactolipid is the same in the wild type and the Su/su mutant, whereas these ratios are twice as high in the yellow mutant Nicotiana tabacum Su/su var. Aurea.The binding of glycolipids and phospholipids onto the subunits of CF1 from Spinacia olera-cea was determined in the Western blot procedure by using monospecific antisera. These experiments lead to the result that the two large subunits (α and β) are marked by antisera to monogalactosyldiglyceride, digalactosyldiglyceride and sulfoquinovosyldiglyceride. The antisera to phospholipids react differently: whereas the antiserum to phosphatidylinositol only reacts with the a-subunit, the antiserum to phosphatidylcholine and that to phosphatidylglycerol react just as the antisera to glycolipids with both large subunits. It is observed that the antiserum to monogalactolipid occasionally marks the y-subunit. This might mean that the glycolipids and the respective phospholipids are tightly bound onto the reacting α-and β-subunits of the CF1-complex. Incubation of the subunit CF1 with lipase from Rhizopus arrhizus and with phospholipase C from Chlostridium perfringens after their transfer to the nitrocellulose membrane abolishes the positive reaction of the peptides with the antisera to glycolipids and phospholipids.
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